N. John Anderson
The Arctic in the twenty-first century: changing biogeochemical linkages across a paraglacial landscape of Greenland
Anderson, N. John; Saros, Jasmine E.; Bullard, Joanna E.; Cahoon, Sean M.P.; McGowan, Suzanne; Bagshaw, Elizabeth A.; Barry, Christopher D.; Bindler, Richard; Burpee, Benjamin T.; Carrivick, Jonathan L.; Fowler, Rachel A.; Fox, Anthony D.; Fritz, Sherilyn C.; Giles, Madeleine E.; Hamerlik, Ladislav; Ingeman-Nielsen, Thomas; Law, Antonia C.; Mernild, Sebastian H.; Northington, Robert M.; Osburn, Christopher L.; Pla-Rab�s, Sergi; Post, Eric; Telling, Jon; Stroud, David A.; Whiteford, Erika J.; Yallop, Marian L.; Yde, Jacob C.
Authors
Jasmine E. Saros
Joanna E. Bullard
Sean M.P. Cahoon
Suzanne McGowan
Elizabeth A. Bagshaw
Christopher D. Barry
Richard Bindler
Benjamin T. Burpee
Jonathan L. Carrivick
Rachel A. Fowler
Anthony D. Fox
Sherilyn C. Fritz
Madeleine E. Giles
Ladislav Hamerlik
Thomas Ingeman-Nielsen
Antonia C. Law
Sebastian H. Mernild
Robert M. Northington
Christopher L. Osburn
Sergi Pla-Rab�s
Eric Post
Jon Telling
David A. Stroud
Erika J. Whiteford
Marian L. Yallop
Jacob C. Yde
Abstract
The Kangerlussuaq area of southwest Greenland encompasses diverse ecological, geomorphic, and climate gradients that function over a range of spatial and temporal scales. Ecosystems range from the microbial communities on the ice sheet and moisture-stressed terrestrial vegetation (and their associated herbivores) to freshwater and oligosaline lakes. These ecosystems are linked by a dynamic glacio-fluvial-aeolian geomorphic system that transports water, geological material, organic carbon and nutrients from the glacier surface to adjacent terrestrial and aquatic systems. This paraglacial system is now subject to substantial change because of rapid regional warming since 2000. Here, we describe changes in the eco- and geomorphic systems at a range of timescales and explore rapid future change in the links that integrate these systems. We highlight the importance of cross-system subsidies at the landscape scale and, importantly, how these might change in the near future as the Arctic is expected to continue to warm.
Citation
Anderson, N. J., Saros, J. E., Bullard, J. E., Cahoon, S. M., McGowan, S., Bagshaw, E. A., Barry, C. D., Bindler, R., Burpee, B. T., Carrivick, J. L., Fowler, R. A., Fox, A. D., Fritz, S. C., Giles, M. E., Hamerlik, L., Ingeman-Nielsen, T., Law, A. C., Mernild, S. H., Northington, R. M., Osburn, C. L., …Yde, J. C. (in press). The Arctic in the twenty-first century: changing biogeochemical linkages across a paraglacial landscape of Greenland. Bioscience, 67(2), https://doi.org/10.1093/biosci/biw158
Journal Article Type | Article |
---|---|
Acceptance Date | Nov 9, 2016 |
Online Publication Date | Feb 1, 2017 |
Deposit Date | Sep 26, 2017 |
Publicly Available Date | Sep 26, 2017 |
Journal | BioScience |
Print ISSN | 0006-3568 |
Electronic ISSN | 1525-3244 |
Publisher | Oxford University Press |
Peer Reviewed | Peer Reviewed |
Volume | 67 |
Issue | 2 |
DOI | https://doi.org/10.1093/biosci/biw158 |
Keywords | tundra, lake, carbon, permafrost, aeolian |
Public URL | https://nottingham-repository.worktribe.com/output/836821 |
Publisher URL | https://academic.oup.com/bioscience/article-lookup/doi/10.1093/biosci/biw158 |
Contract Date | Sep 26, 2017 |
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